Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 2.5–3.5
What and where is it? Dense, 2-5 foot thick slabs exist on most slopes. The weak layers (crusts and weak, sugary faceted snow) are most suspect on W-NW-N-NE-E-SE facing slopes at middle and upper elevations (near and above ~8500' in this zone), but more recently buried rain and sun crusts exist on most middle and upper elevation slopes.
How can you recognize it? Assume the slab + weak layer setup exists on all slopes. Now is not the time to try to outsmart the snowpack. Expect to experience obvious signs of instability—snowpack collapsing and cracks shooting out from your skis or sled—in many areas.
How can you manage it? Sadly, today's answer is "stay off of, away from, and out from beneath all steep slopes." This zone received 5-7" of water (50-70" of dense snowfall) in the past week; there is little to no margin for error today. Natural avalanches are possible, and slides can be triggered remotely—from flat terrain below, above, and to the sides of steep slopes. You could be on flat ground hundreds or thousands of feet below an avalanche starting zone and still trigger an avalanche that reaches you and your travel partners.
(12/20/2025) A large natural avalanche on a north facing slope at 8700ft up Beaver Creek in the Western Smokys.
Photo: Jeremy Lato